MICROSCOPIC DEFORMATION MECHANISM OF GRANULAR MATERIAL IN SIMPLE SHEAR
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概要
- 論文の詳細を見る
rights: 社団法人地盤工学会rights: 本文データは学協会の許諾に基づきCiNiiから複製したものであるrelation: IsVersionOf: http://ci.nii.ac.jp/naid/110003913454/The deformation of granular material was simulated by an assembly of cylinders (made of photoelastic material) packed at random in a two-dimensional simple shear apparatus. From the detailesd observations on the change of granular fabric due to shear, and from the analyses of interparticle contact force among grains, we obtained some experimental facts which must be taken into account in proposing a granular model of sand.With the increase of shear stress in the simple shear test and direct shear test, the normals N_i to the contact planes tend to concentrate toward the maximum principal stress axis. This tendency of the concentration of N_i is not determined by the magnitude of applied shear displacement but by the intensity of mobilized stress ratio τ/σ_N. The preferred direction of N_i gradually rotates with the rotation of principal stress axes during shear deformation. The sliding in microscopic scale at contact is, at any one instant, confined at some preferred contacts. According to the microscopic study of granular fabric of sand deformed in the direct shear apparatus, the similar characters are also observed.
- 社団法人地盤工学会の論文
- 1974-12-15
著者
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小田 匡寛
Dept. Of Foundation Engineering Faculty Of Engineering Saitama University
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小田 匡寛
Department Of Foundation Engineering Saitama University
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小西 純一
Shinshu University
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小西 純一
Department of Civil Engineering, Shinshu University
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小西 純一
Department Of Civil Engineering Shinshu University
関連論文
- ELASTIC COMPLIANCE FOR ROCK-LIKE MATERIALS WITH RANDOM CRACKS
- ELASTIC COMPLIANCE FOR ROCK-LIKE MATERIALS WITH RANDOM CRACKS
- FABRIC TENSOR FOR DISCONTINUOUS GEOLOGICAL MATERIALS
- 浅い基礎の支持力問題における進行性破壊の意味
- On the Influence of Progressive Failure on the Bearing Capacity of Shallow Foundations in Dense Sand(ディスカッション)
- 単純セン断試験におけるτ/σ_N=κ・tanψ関係について
- 単純セン断試験における砂のストレス・ダイレイタンシー関係について
- ON THE RELATION τ/σ_N=κ・tanψ IN THE SIMPLE SHEAR TEST
- CO-ORDINATION NUMBER AND ITS RELATION TO SHEAR STRENGTH OF GRANULAR MATERIAL
- 粒状体材料の一つの力学的・統計的モデル
- ON THE RELATION τ/σ_N=κ・tanψ IN THE SIMPLE SHEAR TEST
- ON STRESS-DILATANCY RELATION OF SAND IN SIMPLE SHEAR TEST
- A MICROSCOPIC STUDY ON SHEAR MECHANISM OF GRANULAR MATERIALS
- 三軸圧縮試験における砂の変形メカニズム
- THE MECHANISM OF FABRIC CHANGES DURING COMPRESSIONAL DEFORMATION OF SAND
- 圧縮変形による構造変化のメカニズム
- 粒状体としての砂の構造および力学的性質と構造との関係について
- INITIAL FABRICS AND THEIR RELATIONS TO MECHANICAL PROPERTIES OF GRANULAR MATERIAL
- A MECHANICAL AND STATISTICAL MODEL OF GRANULAR MATERIAL
- DEFORMATION MECHANISM OF SAND IN TRIAXIAL COMPRESSION TESTS
- THE MECHANISM OF FABRIC CHANGES DURING COMPRESSIONAL DEFORMATION OF SAND
- EFFECT OF STRENGTH ANISOTROPY ON BEARING CAPACITY OF SHALLOW FOOTING IN A DENSE SAND
- EXPERIMENTAL STUDY OF ANISOTROPIC SHEAR STRENGTH OF SAND BY PLANE STRAIN TEST
- STRESS-INDUCED ANISOTROPY IN GRANULAR MASSES
- ROTATION OF PRINCIPAL STRESSES IN GRANULAR MATERIAL DURING SIMPLE SHEAR
- MICROSCOPIC DEFORMATION MECHANISM OF GRANULAR MATERIAL IN SIMPLE SHEAR
- A MICROSCOPIC STUDY ON SHEAR MECHANISM OF GRANULAR MATERIALS
- SHEAR STRENGTH OF UNDISTURBED SAMPLE OF DECOMPOSED GRANITE SOIL
- マサ土の乱さない試料のセン断強度(『土質工学会論文報告集』Vol.16,No.1(1976年3月発行)掲載論文の概要)
- SHEAR STRENGTH OF UNDISTURBED SAMPLE OF DECOMPOSED GRANITE SOIL
- THE EFFECT OF CRACK GEOMETRY ON HYDRODYNAMIC DISPERSION IN CRACKED MEDIA
- INITIAL FABRICS AND THEIR RELATIONS TO MECHANICAL PROPERTIES OF GRANULAR MATERIAL